Sea-level and ocean-current control on carbonate-platform growth, Maldives, Indian Ocean
Author:
Affiliation:
1. Department of Geosciences; University of Hamburg; Hamburg; Germany
2. Department of Sedimentology and Marine Geology; VU University Amsterdam; Amsterdam; The Netherlands
3. Department of Earth Science MS-126; Rice University; Houston; TX; USA
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2117.2012.00554.x/fullpdf
Reference65 articles.
1. SONIC VELOCITY IN CARBONATES—A COMBINED PRODUCT OF DEPOSITIONAL LITHOLOGY AND DIAGENETIC ALTERATIONS
2. From the Great Bahama Bank into the Straits of Florida: a Margin Architecture Controlled by Sea-Level Fluctuations and Ocean Currents;Anselmetti;Geol. Soc. Am. Bull.,2000
3. General cenozoic evolution of the Maldives carbonate system (equatorial Indian Ocean);Aubert;Bull. Centres Rech. Explor.-Prod. Elf-Aquitaine,1992
4. Seismic stratigraphy and depositional signatures of the Maldive carbonate system (Indian Ocean);Aubert;Mar. Pet. Geol.,1996
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